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DYNAMICS OF COLORED DISSOLVED ORGANIC MATTER IN THE CLIMATE CHANGING ENVIRONMENT OF NORTHERN SIBERIA

机译:西北地区气候变化环境中有色溶解有机物的动态变化

摘要

The Lena is one of the largest rivers in the world and is responsible, through its outflow to the Laptev Sea, for a significant fraction of the total fresh water and organic matter discharge into the Arctic Ocean. With the known effects of climate change in the Arctic and associated increase of permafrost thaw rates, the Lena River discharge and consequent export of terrigenous dissolved organic matter (DOM) into the Arctic Ocean tends to increase. Such variations may affect the nutrients and carbon dynamics in the region with consequences for the primary production and the CO2 exchanges in the ocean-atmosphere boundary layer. Understanding the dynamics and optical properties of colored DOM (CDOM) is of great value for carbon cycle modelling since CDOM is the fraction of the DOM which interacts with light and can be detected by satellite ocean color remote sensing. In this context, this study aims to investigate the dynamics of CDOM regarding the hydrographical forcing in the Lena Delta region based on in situ data collected during the late summer 2013. Water column structure was assessed through temperature and salinity profiles acquired with CTD casts and the CDOM characterization and quantification were determined based on both absorption and fluorescence spectra obtained with a HORIBA© Aqualog spectrofluorometer. The CDOM absorption at 443nm (a443; used as a CDOM amount index) and the terrestrial and marine absorption slopes of CDOM [STER (275-295nm) and SMAR (350-400nm), respectively] were obtained based on the absorption spectra. The CDOM components were identified by analysis of the excitation-emission-matrices and based on the literature. a443 was directly (inversely) related with temperature (salinity), denoting the strong modulation of CDOM by the hydrographical forcing: the highest CDOM amounts with riverine compounds were related to the Lena River Plume, while the salty waters from Laptev Sea presented lower a443 and associated with marine compounds.
机译:莉娜河是世界上最大的河流之一,并通过流入拉普捷夫海的原因,负责向北冰洋排放的淡水和有机物总量的很大一部分。随着北极地区气候变化的已知影响以及永久冻土融化速率的增加,勒纳河的排放量以及随之而来的向北冰洋的陆源溶解性有机物(DOM)的出口趋于增加。这种变化可能影响该区域的养分和碳动态,从而影响海洋-大气边界层的初级生产和二氧化碳交换。了解彩色DOM(CDOM)的动力学和光学特性对于碳循环建模具有重要价值,因为CDOM是DOM中与光相互作用的部分,可以通过卫星海洋颜色遥感进行检测。在此背景下,本研究旨在基于2013年夏末收集的原位数据,调查有关莉娜三角洲地区水文强迫的CDOM动力学。通过使用CTD铸件和冰壳获得的温度和盐度剖面评估水柱结构。基于使用HORIBA©Aqualog分光荧光计获得的吸收光谱和荧光光谱,确定CDOM的表征和定量。基于吸收光谱,获得了在443nm处的CDOM吸收(a443;用作CDOM量指标)以及CDOM的陆地和海洋吸收斜率[分别为STER(275-295nm)和SMAR(350-400nm)]。通过对激发-发射矩阵的分析并根据文献确定了CDOM成分。 a443与温度(盐度)直接(成反比),表明水文强迫对CDOM的强烈调节:含河化合物的最高CDOM量与莉娜河羽有关,而拉普捷夫海的咸水含量较低,而a443和与海洋化合物有关。

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